North Bay Resources Inc (NBRI)

[mick]

#42/\08-26-2019/ Technical Assessment Report on the Mount Washington Property
http://www.northbayresources.com/2019_MW_43101.pdf

Vancouver Island, British Columbia
NTS 092F/14
BCGS 092F074 & 092F075
Latitude 490 45’ 23” Longitude 1250 15’ 22”
UTM NAD83 Zone 10N 337500E 5514000N
For
North Bay Resources Inc.
PO Box 162
Skippack, PA, USA 19474
By
Jacques Houle P.Eng.
6552 Peregrine Road
Nanaimo, B.C. V9V 1P8
August 26, 2019
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through wide but variably mineralized sections using consistent 10’ (3.0 m.) sample intervals,
regardless of variations in the lithology, or the amount and type of mineralization. Such
sampling could blur contacts between higher grade and lower grade sections intersected, and
cause grades of higher-grade sections to be under-stated. Also, there are examples in trench
and rock sampling records of samples exceeding the analytical limits in a metal of economic
interest, say >10,000 ppm. or >1% copper using atomic absorption methods, for which no
follow-up assays are available. This could result in grades of some zones to be understated as
well. In the History section, the author has converted all of the units to metric formats,
precious metal analyses to grams per tonne, and base metal analyses to percentages (unless
very low) for consistency within the report, and with current industry standards.
Since the last significant exploration programs occurred on the Mount Washington Property in
1992, prices for target commodities gold, silver, copper, molybdenum and tellurium have
greatly increased. The understanding of mineral deposits by economic geologists has improved
substantially, and the exploration techniques used have improved dramatically. In addition,
the property has been the focus of several academic geology papers by qualified geoscientists,
including highly experienced government personnel. The understanding of mineral deposits by
economic geologists has improved substantially since the last exploration and academic work
was done in the Property area. The bulk sampling program completed in 2009 and the tailings
sampling program completed in 2011 by Clibetre Explorations Ltd. were implemented primarily
to fulfill mineral tenure requirements, but the limited work completed was done to modern
industry standards. In 2013, the author completed a preliminary field work program on the
Property for North Bay Resources Inc., consisting of re-locating and sampling of selected,
known and accessible mineralized occurrences in outcrops. In 2016, the author commenced a
detailed field work program on the Murex Breccia, consisting of geological mapping and
selected sampling of mineralized occurrences in outcrop. In early 2018, the author engaged
Auracle Remote Sensing Inc. of Qualicum Beach, BC to acquire and fuse radarsat data for the
area of the Mt. Washington Property on behalf of North Bay Resources Inc. In 2018, the author
continued the detailed work program on the Murex Breccia, including soil geochemistry as well.
These work programs were implemented to both fulfill mineral title requirements as well as to
document, verify and enhance the knowledge of various settings, styles, and grades of those
mineralized occurrences.
On June 4, 2019, the author submitted a Section 19 Notice to surface rights owner TimberWest
on behalf of North Bay Resources Inc., including a map shown in Figure 3 showing possible 2019
field program locations in the Murex and Wolf Lake areas. The actual 2019 work area along
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with those from 2016 and 2018 are shown in Figure 4. On July 15, 2019 the author and his son,
field technician Adrian Houle mobilized with equipment and supplies from Nanaimo to a rental
apartment in a chalet at the Mount Washington Village. From July 16th to July 18th field
personnel commuted daily by truck from the Mount Washington village to a locked gate at the
beginning of Murex Main logging road along Strathcona Parkway, and cycled for 4 to 5 km.
along Murex Main to access the 2019 work area. Demobilization occurred on July 18th, 2019.
From July 16th to July 18th the author continued the multi-year GPS grid-controlled geological
mapping and selective outcrop rock sampling program in the Murex Breccia Area for North Bay,
shown in Figure 5a. Three days were spent in part by the author conducting outcrop geological
mapping continuing NE on the Murex Breccia Grid along GPS-controlled NW-SE-oriented grid
lines, along available logging road cuts and rock quarries within the grid area, and along Murex
Creek. The approximate perimeters of all visible outcrops seen within the grid area were
recorded onto water proof metric gridded sheets in a field note book at 1:1,000 scale, along
with outcrop elevations, rock types, contacts, structures, alteration and mineralization, as well
as creeks and roads where traversed. At the apartment each evening the day’s mapping was
traced onto gridded vellum paper sheets, so that the field mapping was duplicated for secure
storage at the apartment and original mapping sheets available for use in the field the next day.
Approximately 3.5 line-km of detailed GPS grid-controlled geological mapping was completed,
extending northeast from the area mapped in 2018, with the combined data from 2016, 2018
and 2019 programs combined and shown in part in Figure 5a. Only two different rock types
were mapped in this largely overburden-covered area in 2019, including quartz-sulphide veins
hosted in volcanics and in volcanic breccias, summarized as follows:
? Mafic Volcanic Breccia (MVBx) – matric-supported, fine grained, sulphidic polymictic
breccia with fine grained mafic volcanic matrix containing quartz-sulphide stockwork
veins and occurring along Murex Creek in the north-west portion of the mapped area,
and along Murex Main road in the north-central portion of the mapped area
? Mafic Volcanic (MV) – fine grained, massive, pillowed to flow-brecciated, variably
sulphidic mafic volcanic containing quartz-sulphide veins occurring along Murex Creek
where Murex Main road meets Tsolum Main road (site of removed bridge)
Narrow (0.25 to 0.05 m. thick) banded quartz-sulphide veins were observed in outcrops of
mafic volcanics, and thicker (up to 5 m. thick) quartz-sulphide stockwork zones were observed

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